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Published online 21 June 2006
Published in Vadose Zone J 5:815-823 (2006)
DOI: 10.2136/vzj2005.0119
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Irrigating Forage Crops with Saline Waters

1. Volumetric Lysimeter Studies

T. H. Skaggs*, J. A. Poss, P. J. Shouse and C. M. Grieve

George E. Brown, Jr., Salinity Lab., USDA-ARS, 450 W. Big Springs Rd., Riverside, CA 92507

Figure 1
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Fig. 1. Schematic diagram of a volumetric lysimeter. The experiment was conducted in a facility consisting of 24 lysimeters.

 

Figure 2
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Fig. 2. Illustration of the calculation of irrigation and drainage depths based on measurements of reservoir water height.

 

Figure 3
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Fig. 3. Measured evapotranspiration (ET) in two well-watered lysimeters, expressed as the ratio of the measured ET to a reference ET0 calculated using a modified Penman equation.

 

Figure 4
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Fig. 4. Phase 1 measured relative yields as a function of the electrical conductivity (salinity) of the irrigation water (ECiw). Data are cumulative totals collected during five harvests. The shaded areas represent the range of yields expected based on published salt tolerances.

 

Figure 5
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Fig. 5. Phase 1 measured yields as a function of the electrical conductivity (salinity) of the irrigation water (ECiw). Date are the same as in Fig. 4, except in absolute instead of relative terms.

 

Figure 6
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Fig. 6. Observed relationship between relative yield and relative evapotranspiration as measured in the Phase 1 experiments. Ky is the yield response factor and ECiw is the electrical conductivity of the irrigation water.

 

Figure 7
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Fig. 7. Measured leaching fraction as a function of irrigation depth and electrical conductivity (salinity) of the irrigation water (ECiw). Data are from Phase 2 and are 50-d cumulative totals.

 

Figure 8
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Fig. 8. Time variation of the drainage water salinity (ECdw) measured in selected alfalfa lysimeters during Phase 1. The dashed lines are steady-state model calculations.

 





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